Main Features of the Permian Halogenesis Hydrochemistry in the Caspian Region

Moskovsky, Georgiy Aleksandrovich; Гончаренко, О. П.; Svidzinskiy, Sergey Alekandrovich

doi:10.18500/1819-7663-2011-11-1-69-75

2011

DOI: 10.18500/1819-7663-2011-11-1-69-75

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Main Features of the Permian Halogenesis Hydrochemistry in the Caspian Region

Georgiy Aleksandrovich Moskovsky¹,

О. П. Гончаренко²,

Sergey Alekandrovich Svidzinskiy³

Abstract: 21. Хаин В.Е. Крупномасштабная цикличность в тектонической истории Земли и ее возможные причины // Геотектоника. 2000. № 6. С. 3-14. 22. Алексеев А.С. Глобальные биотические кризисы и массовые вымирания в фанерозойской истории Земли // Биотические события на основных рубежах фанерозоя.

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Paleohydrogeology of the Anabar-Khatanga Basin

Черных¹,

Novikov²

2018

Oil and Gas Studies

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The hydrogeological history of the Anabar-Khatanga basin covers the period from the Archaean to the Quaternary and includes 12 hydrogeological cycles. The Jurassic-Eopleistocene cycle is the longest during which there were continental conditions of sedimentation with the longest infiltration stage (from the Lower Cretaceous to the Neo-Pleistocene). The salts of the Devonian salt basin play a key role in the formation of the groundwater and brines composition within the following structures: Nordvik, Southern Tigyan, Ilya Kozhevnikova, Ledovka and Belaya.

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Paleohydrogeology of the Anabar-Khatanga Basin

Черных¹,

Novikov²

2018

Oil and Gas Studies

View full text Add to dashboard Cite

show abstract

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Main Features of the Permian Halogenesis Hydrochemistry in the Caspian Region

Cited by 1 publication

References 0 publications

Paleohydrogeology of the Anabar-Khatanga Basin

Paleohydrogeology of the Anabar-Khatanga Basin

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